Zobrazeno 1 - 10
of 57
pro vyhledávání: '"Reidulv Bøe"'
Publikováno v:
GEUS Bulletin, Vol 52, Pp 1-16 (2022)
Geology is a core component of two major multidisciplinary seabed-mapping initiatives in Norway (MAREANO, Marine Base Maps for the Coastal Zone). Helped by Norway’s Nature Diversity Act, which acknowledges geological and landscape diversity alongsi
Externí odkaz:
https://doaj.org/article/3e4e92fbe2364fdaaeb5288d0ddb6487
Publikováno v:
Journal of Maps, Vol 15, Iss 2, Pp 686-696 (2019)
An increasing number of activities compete for space in the Norwegian coastal zone, making access to detailed seabed information particularly valuable. We present a suite of thematic marine base maps of the near-shore areas of five municipalities in
Externí odkaz:
https://doaj.org/article/b768d66d97614afdbc28669efa062694
Autor:
Jochen Knies, Denizcan Köseoğlu, Leif Rise, Nicole Baeten, Valérie K. Bellec, Reidulv Bøe, Martin Klug, Giuliana Panieri, Patrycja E. Jernas, Simon T. Belt
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
Polynyas potentially played a role in sustaining marine life during the last glacial, yet their presence and importance remains equivocal. This multi-proxy study reconstructs a corridor of polynyas in the Nordic Seas during the last glacial maximum,
Externí odkaz:
https://doaj.org/article/6670dc4b31a64320bced92848cb27c52
Autor:
Valérie K. Bellec, Reidulv Bøe, Leif Rise, Aave Lepland, Terje Thorsnes, Lilja Rún Bjarnadóttir
Publikováno v:
Journal of Maps, Vol 13, Iss 2, Pp 608-620 (2017)
This paper presents a seabed sediments (grain size) map of the Nordland VI area (25,000 km2) off the Lofoten islands, north Norway. The map is based on multibeam echosounder data (bathymetry and backscatter), visual analysis of 215 video transects (e
Externí odkaz:
https://doaj.org/article/45e317d0e9d046f784ab81aeffd4a220
Recently, international focus on the United Nations Sustainable Development Goals has led to the proposal of Essential Geodiversity Variables (EGVs), a framework for geological (geodiversity) information, intended to stand alongside Essential Variabl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::280213909dfd76192acec46e34660f90
https://doi.org/10.5194/egusphere-egu23-5129
https://doi.org/10.5194/egusphere-egu23-5129
The Hølonda area of the central Scandinavian Caledonides is a key for models of the Caledonian orogen owing to its Ordovician fauna of Laurentian affinity, now stranded on the Baltic side during opening of the North Atlantic. Here, we present a revi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e56dfd6d9b981754ec9e752ed60f463
Autor:
Terje Thorsnes, Oddvar Longva, Sigrid Elvenes, Aave Lepland, Margaret F.J. Dolan, Lilja Rún Bjarnadóttir, Reidulv Bøe, Valérie K. Bellec
Publikováno v:
Geological Society, London, Special Publications. 505:57-69
Results from geological mapping within the MAREANO (Marine Areal Database for Norwegian Coasts and Sea Areas) programme and mapping projects in the coastal zone reveal a rich and diverse seafloor in Norwegian territories. The geomorphology and sedime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f555e8bf3e7b0f3f7bae0f36ca56ee6
https://doi.org/10.1144/sp505-2019-82
https://doi.org/10.1144/sp505-2019-82
Publikováno v:
Norwegian Journal of Geology. 100:1-24
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6dd76697b20136a307746b897120d55d
https://doi.org/10.17850/njg100-1-3.
https://doi.org/10.17850/njg100-1-3.
Publikováno v:
Palaeoworld
The late Early to early Middle Ordovician Fjellvollen Formation, Central Norwegian Caledonides, is a part of the Ilfjellet Group volcano-sedimentary succession formed in a rift basin that opened along the Laurentian margin. Depositional facies and tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7a25a06144568650c212eb9657642e8
https://hdl.handle.net/11250/3060481
https://hdl.handle.net/11250/3060481
Publikováno v:
Geological Society of America Bulletin
Arc-continent collision, followed by subduction polarity flip, occurs during closure of oceanic basins and contributes to the growth of continental crust. Such a setting may lead to a highly unusual association of ultrapotassic and mid-ocean ridge ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2db73c3f00522220539eed1d5d3cc68d
http://hdl.handle.net/10852/91935
http://hdl.handle.net/10852/91935